Quantitative estimate of the Milankovitch-forced contribution to observed Quaternary climate change
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Penultimate deglacial sea-level timing from uranium/thorium dating of Tahitian corals.Biological early diagenesis and insolation-paced paleoproductivity signified in deep core sediment organic matter.Obliquity pacing of the late Pleistocene glacial terminations.Testing competing forms of the Milankovitch hypothesis: A multivariate approach
P2860
Quantitative estimate of the Milankovitch-forced contribution to observed Quaternary climate change
description
article
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im Mai 2004 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в травні 2004
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ലേഖനം
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name
Quantitative estimate of the M ...... rved Quaternary climate change
@en
Quantitative estimate of the M ...... rved Quaternary climate change
@nl
type
label
Quantitative estimate of the M ...... rved Quaternary climate change
@en
Quantitative estimate of the M ...... rved Quaternary climate change
@nl
prefLabel
Quantitative estimate of the M ...... rved Quaternary climate change
@en
Quantitative estimate of the M ...... rved Quaternary climate change
@nl
P1476
Quantitative estimate of the M ...... rved Quaternary climate change
@en
P2093
Carl Wunsch
P304
P356
10.1016/J.QUASCIREV.2004.02.014
P577
2004-05-01T00:00:00Z